Mixed Solution and Equilibrium Challenge
Concentration conversion followed by reaction quotient
Lesson 2472 of 4,500 · Physical Chemistry Problem Solving
Learning objectives
- Convert mass-fraction and density data into molar concentrations
- Recalculate every concentration after two solutions are mixed
- Compare the reaction quotient with the equilibrium constant to predict the direction of change or precipitation
Introduction
Equilibrium questions in the laboratory rarely start with neat concentrations at equilibrium. Instead you are given a stock solution labelled by mass percent and density, or two solutions that are poured together. Before any equilibrium reasoning is possible, every species must be expressed as a concentration in the final mixture. This page links concentration conversion to the reaction quotient Q, the tool that tells you which way a mixture will move.
Core explanation
Stage 1: convert to molarity. A solution labelled with mass fraction w and density ρ is most easily handled by taking a basis of 1 dm³ (1000 cm³). The mass of solution is 1000ρ grams (ρ in g/cm³), the mass of solute is w × 1000ρ, and dividing by the molar mass gives moles per dm³. This is the density-based conversion from earlier in the unit, used here as the first link in a chain.
Stage 2: account for mixing. When volumes V₁ and V₂ are mixed, the total volume is usually taken as V₁ + V₂ for dilute aqueous solutions. Every species in each solution is diluted: c(new) = c(old) × V(old)/V(total). A frequent error is to dilute only one of the two solutions or to forget that spectator ions are diluted as well. Moles are conserved on mixing; concentrations are not.
Stage 3: react anything that goes essentially to completion. If the mixture contains a strong acid and a strong base, or another reaction with a very large K, deal with that stoichiometrically first, using moles. Only the leftover amounts are used in the equilibrium stage.
Stage 4: evaluate Q. Q has exactly the same form as K but uses the current concentrations. Then compare:
- Q < K: the reaction proceeds forward, forming more products. - Q > K: the reaction proceeds in reverse. - Q = K: the mixture is already at equilibrium.
For a sparingly soluble salt, Q is the ion product. For PbCl₂(s) ⇌ Pb²⁺(aq) + 2Cl⁻(aq), Q = [Pb²⁺][Cl⁻]². If Q exceeds Ksp, the solution is supersaturated and a precipitate is expected; if Q is below Ksp, all the salt stays dissolved. Note that solids and the solvent do not appear in Q.
Formulae
c = (1000 × ρ × w)/M in mol/dm³ (ρ in g/cm³). c(mixed) = c × V/V(total). Q = Πcᵢ^νᵢ (products over reactants, each raised to its coefficient).
Step-by-step reasoning
1. Convert every stock solution into mol/dm³. 2. Find the total volume after mixing and dilute every species. 3. Carry out any complete reaction using moles, then return to concentrations. 4. Write the Q expression from the balanced equation. 5. Substitute and compare Q with K or Ksp, and state the direction.
Visual explanation
Draw a horizontal number line of the value of Q with K marked on it. Mixtures to the left of K move right, towards products; mixtures to the right move left. Mixing two solutions places the starting point somewhere on the line, and dilution slides it, sometimes across K.
Real-world analogy
Q is like checking your bank balance against a target before deciding to save or spend. The number you compare must be today's balance after all the latest deposits and withdrawals, just as Q must use concentrations after mixing and dilution, not the values printed on the original bottles.
Real-world example
Water-treatment chemists predict scale formation by comparing the ion product of calcium and carbonate ions in a blended water supply with the Ksp of calcium carbonate. Mixing a hard groundwater with a softer surface water changes both concentrations, and the blend may or may not deposit scale in pipes.
Why?
Why must concentrations be recalculated after mixing? K is defined in terms of the concentrations actually present in the final solution. Adding volume lowers every concentration, and because Q multiplies powers of concentrations, a dilution can change Q by a large factor, especially when coefficients are greater than one.
Common misconception
"If both solutions contain the ions needed, a precipitate must form." Precipitation happens only when the ion product exceeds Ksp. Dilute solutions can be mixed with no visible change at all.
Worked example
Question: 20.0 cm³ of 0.0100 mol/dm³ Pb(NO₃)₂ is mixed with 30.0 cm³ of 0.0200 mol/dm³ NaCl. Ksp(PbCl₂) is about 1.7 × 10⁻⁵ at 25 °C. Does a precipitate form?
Reasoning: Total volume = 50.0 cm³. [Pb²⁺] = 0.0100 × 20.0/50.0 = 4.00 × 10⁻³ mol/dm³. [Cl⁻] = 0.0200 × 30.0/50.0 = 1.20 × 10⁻² mol/dm³. Q = (4.00 × 10⁻³)(1.20 × 10⁻²)² = 5.8 × 10⁻⁷. This is well below Ksp.
Answer: Q < Ksp, so no precipitate of PbCl₂ forms.
Quick check
1. A solution of ethanoic acid is 6.00% by mass with density 1.007 g/cm³. What is its concentration in mol/dm³ (M = 60.05 g/mol)? Answer: 1000 × 1.007 × 0.0600 = 60.4 g per dm³, which is 60.4/60.05 ≈ 1.01 mol/dm³.
Exam focus
Examiners reward a clear statement of the total volume, the diluted concentration of each ion, the correct Q expression with powers, and a verbal conclusion comparing Q with K. Remember that the stoichiometric coefficient becomes a power, so [Cl⁻] is squared for PbCl₂.
Advanced insight
At higher ionic strength, activities replace concentrations and are smaller than the concentrations, so a simple ion-product calculation can overestimate the tendency to precipitate. Close to the boundary Q ≈ Ksp, supersaturated solutions can also persist for some time because forming the first crystal nuclei is kinetically slow.
Summary
Mixed-solution equilibrium problems are chains: convert mass fraction and density into molarity, dilute every species to the total volume, remove any complete reactions stoichiometrically, and then evaluate Q. Comparing Q with K predicts the direction of change, and comparing the ion product with Ksp predicts whether a precipitate forms.
Practice questions
1. 10.0 cm³ of 0.100 mol/dm³ AgNO₃ is mixed with 90.0 cm³ of 1.0 × 10⁻⁴ mol/dm³ NaCl. Ksp(AgCl) ≈ 1.8 × 10⁻¹⁰. Does AgCl precipitate? Answer: [Ag⁺] = 0.0100 and [Cl⁻] = 9.0 × 10⁻⁵ mol/dm³, so Q = 9.0 × 10⁻⁷, which exceeds Ksp; a precipitate forms. 2. A reaction A + B ⇌ C has K = 50. After mixing, [A] = 0.10, [B] = 0.20 and [C] = 2.0 mol/dm³. Which way does it move? Answer: Q = 2.0/(0.10 × 0.20) = 100, which is greater than K, so the reaction moves in reverse. 3. Why does doubling the volume of a mixture by adding water change Q for A + B ⇌ C but not for A ⇌ B? Answer: For A ⇌ B, both concentrations halve and the ratio is unchanged; for A + B ⇌ C, Q doubles because the denominator has two concentration terms. 4. Why are spectator ions such as nitrate left out of Q for PbCl₂ precipitation? Answer: They do not appear in the dissolution equilibrium, so they do not enter the equilibrium expression, although they still affect the total volume and ionic strength.